Abstract
Abstract: Berijam lake, Tamil Nadu, situated at an elevation of 2165 m above mean sea level is a fresh water, irregular linear basin with two major linear arms located in the Palani hills. Lake floor sediments were collected covering the entire aerial extent of this lake basin to understand the sediment pattern distribution and plausible source of organic carbon. Textural pattern, CaCO3, Organic matter, TOC, TN content and the C/N ratio of the lake floor sediment samples were analysed and the data generated exhibit a distinct pattern of sediment distribution and deposition. Grain size data indicate that the clay is associated with both sand and silt and the lake is dominantly composed of sandy clay and silty clay. CaCO3 content is low (2.70 to 0.80%) as there is no major source for CaCO3. OM, TOC and TN show positive correlation with silt. C/N ratio varies from (12.2 to 9.6) indicating dominantly algal organic matter. NNW, NNE and SSE region of the lake seems to have supported thick water column as high organic carbon, silt and clay content occur in these directions. C/N ratio indicates that the major source of organic matter is from the lake algae, aquatic weeds and plants.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
